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White Sands lies in the Tularosa Basin. The gypsum that forms the white sands was deposited at the bottom of a shallow sea that covered the region 250 million years ago during the Permian era. Over time the gypsum-bearing marine deposits like the Yeso and San Andres formations were turned into stone.
The basin lies between the San Andres Mountains (west) and the Sacramento Mountains (east). The sand constantly drifts into dunes 10 to 60 feet (3 to 18 metres) high.
The park not only contains the large dune field but also a saline mudflat called Alkali Flat, a smaller ephemeral salt lake (or playa) named Lake Lucero, parts of the gypsum-dust plains east of the dune field, and alluvial fans from the surrounding mountains.
Lake Lucero is a dry lake bed that only fills with water when there has been abundant rain or snow in the surrounding area.
The story of the worlds largest gypsum dunefield began 280 million years ago when the Permian Sea covered this area and gypsum settled on the sea floor. The formation of the dunefield continues today in an endless cycle of erosion and renewal.
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Dunes are mounds of loose sand created by wind and are the most well known aeolian features. There are a varitety of types of dunes, depending on their shape. Most dunes share a common profile, or cross section, with a long shallow angle (stoss) facing into the wind, a peak (crest), and a steep lee side.
White Sands National Park offers a ranger-led tour of Lake Lucero for visitors interested in learning more about the formation of the dunes and the origin of the sands.
Major geomorphic features of the area include extensive floors of intermontane basins, such as the Tularosa Basin; contiguous piedmont slopes, or bajada; and upland areas, including mountain ranges (e.g., San Andes and Sacramento) and high plateaus, with steep bounding escarpments.

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